Extended Data Fig. 2: Sensitivity analysis of the applied corrections.
From: Global sea-level rise in the early Holocene revealed from North Sea peats
The vertical position and uncertainty of each SLIP was calculated using correction steps for background subsidence, palaeotidal changes and compaction. Calculation of calibrated age and uncertainty (horizontal axis) included a Bayesian step. The curves and dashed envelopes show the rates when excluding one or all of the steps, besides the all-inclusive run (black line, pink envelope; as in main text). Each correction step has impact, but even without any correction the double peak in the rates remains.
